Differential impacts of nitrogen addition on rhizosphere and bulk‐soil carbon sequestration in an alpine shrubland

Due to complex root–soil interactions, the responses of carbon (C) dynamics in the rhizosphere to elevated nitrogen (N) deposition may be different from those in bulk soil. However, the potentially different response of C dynamics in the rhizosphere and bulk soils and their contributions to soil C sequestration under N deposition is still not elucidated. We conducted an N addition experiment in an alpine shrubland dominated by Sibiraea angustata...